How are the crust, mantle, core alike
... 1. How are the crust, mantle, core alike? Different? 2. What is a tectonic plate? 3. What powers the movement of the tectonic plates? Tell where this force is and how it works? 4. What are seismic waves? 5. Why do seismic waves travel at different speeds in the lithosphere, Asthenosphere, mantle out ...
... 1. How are the crust, mantle, core alike? Different? 2. What is a tectonic plate? 3. What powers the movement of the tectonic plates? Tell where this force is and how it works? 4. What are seismic waves? 5. Why do seismic waves travel at different speeds in the lithosphere, Asthenosphere, mantle out ...
The Solar System
... – large pieces of the crust and part of the mantle called the lithosphere • seven very large ones and lots of small ones • constantly moving/floating (116cm/year) on the plastic part of the mantle because of convection currents in the soft rock underneath them –this is called continental drift ...
... – large pieces of the crust and part of the mantle called the lithosphere • seven very large ones and lots of small ones • constantly moving/floating (116cm/year) on the plastic part of the mantle because of convection currents in the soft rock underneath them –this is called continental drift ...
GEOS 110 Fall 2011 Test 2 Study Guide Test cover`s Chapters: 5
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
GEOS 110 Fall 2013 Test 2 Study Guide
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
... 55. In what way is the earth dynamic rather than static for its internal heat, magnetic field, solid mantle, continent configuration and ocean basin shape? 56. Where does melting take place in the Earth? 57. What is the state of the Mantle? 58. Where is new lithosphere made? 59. Where is ocean litho ...
Tectonic Plates Quiz
... e) A discrete layer in the mantle immediately below the crust. 3. Volcanoes and earthquakes are found along… a) all of the edges of all continents. c) some of the edges of all continents. b) all of the edges of some continents. d) some of the edges of some continents. 4. What is the principal cause ...
... e) A discrete layer in the mantle immediately below the crust. 3. Volcanoes and earthquakes are found along… a) all of the edges of all continents. c) some of the edges of all continents. b) all of the edges of some continents. d) some of the edges of some continents. 4. What is the principal cause ...
Geological History
... • Isostasy- The crust floats on the mantle since the crust is less dense. • The heavier the crust, the more it will push on the mantle • Mantle is not “liquid” like we think of it…it has plasticity. ...
... • Isostasy- The crust floats on the mantle since the crust is less dense. • The heavier the crust, the more it will push on the mantle • Mantle is not “liquid” like we think of it…it has plasticity. ...
Unit Test Earth Patterns, Cycles, and Changes Name
... 22. Rocks which formed in areas once covered by oceans often contain fossils of animals which lived in the sea. Which one of these rocks contains fossils of ocean animals? ...
... 22. Rocks which formed in areas once covered by oceans often contain fossils of animals which lived in the sea. Which one of these rocks contains fossils of ocean animals? ...
geodesi fisis - WordPress.com
... The behavior of the earth’s ice masses is critical indicator of global climate change and global sea level behavior. Thus, monitoring of melting of Greenland and Antarctica ice cap is an important issue, the ice cap are huge mass loads, sitting on the earth’s crust, which will necessarily be depress ...
... The behavior of the earth’s ice masses is critical indicator of global climate change and global sea level behavior. Thus, monitoring of melting of Greenland and Antarctica ice cap is an important issue, the ice cap are huge mass loads, sitting on the earth’s crust, which will necessarily be depress ...
4 layers of Earth and Plate Activity notes
... • When plates collide they create mountains this is called a collision zone • Appalachian mountains – Africa collided with North America during formation of Pangea • Destroy sea floor- ocean plates more dense than land plates, when they converge ocean plates slide under land plates ...
... • When plates collide they create mountains this is called a collision zone • Appalachian mountains – Africa collided with North America during formation of Pangea • Destroy sea floor- ocean plates more dense than land plates, when they converge ocean plates slide under land plates ...
study guide – unit 9 – plate tectonics
... Continental “fit” : coastlines match up Rocks, minerals and fossils: similar age and composition ...
... Continental “fit” : coastlines match up Rocks, minerals and fossils: similar age and composition ...
EGU2017-5944
... (1) University College London, London, United Kingdom ([email protected]), (2) Universita di Padova, Padova, Italy ([email protected]), (3) Kangwon National University, Chuncheon, South Korea ([email protected]), (4) University College London, London, United Kingdom (william.sturg ...
... (1) University College London, London, United Kingdom ([email protected]), (2) Universita di Padova, Padova, Italy ([email protected]), (3) Kangwon National University, Chuncheon, South Korea ([email protected]), (4) University College London, London, United Kingdom (william.sturg ...
Plate Tectonics II
... In most other areas, the rocks have fractured in normal faults, which are produced only by stretching a brittle material - pulling it apart. ...
... In most other areas, the rocks have fractured in normal faults, which are produced only by stretching a brittle material - pulling it apart. ...
The Earth*s Physical Geography
... above the surrounding land One steep slope Plains are large areas of flat land, but can also be gently rolling ...
... above the surrounding land One steep slope Plains are large areas of flat land, but can also be gently rolling ...
Lesson 2 Unit Notes
... Unit 2 Changes to the Earth’s Surface Lesson 2 Unit Notes pg. 240-246 13. What can cause Earthquakes? ________________________________________________________________________ ________________________________________________________________________ ___________________________________________________ ...
... Unit 2 Changes to the Earth’s Surface Lesson 2 Unit Notes pg. 240-246 13. What can cause Earthquakes? ________________________________________________________________________ ________________________________________________________________________ ___________________________________________________ ...
Geology Test Study Guide Answers
... also occur. If ocean-ocean plates meet, you can have a valley or ocean trench. Divergent boundaries- when plates move away from one another – sea floor spreading happen, mid-ocean ridges can form. Transform boundaries- plates slide up and down against each other- earthquakes happen Volcanic Mountain ...
... also occur. If ocean-ocean plates meet, you can have a valley or ocean trench. Divergent boundaries- when plates move away from one another – sea floor spreading happen, mid-ocean ridges can form. Transform boundaries- plates slide up and down against each other- earthquakes happen Volcanic Mountain ...
Earth: Chapter 1
... 1. waves break when they reach __________ water a. breaking waves release a tremendous amount of _____; they can ______ and ______________ rock, eventually turning it into _______ C. Waves can create a variety of features along a ____________ 1. sea stacks = offshore columns of _________________ 2. ...
... 1. waves break when they reach __________ water a. breaking waves release a tremendous amount of _____; they can ______ and ______________ rock, eventually turning it into _______ C. Waves can create a variety of features along a ____________ 1. sea stacks = offshore columns of _________________ 2. ...
Introduction to Earthquakes EASA
... Since new material is created at the mid-ocean ridges and Earth is not expanding, somewhere material must be removed from the surface. It turns out that old ocean floor is “subducted” into the mantle at subduction zones. ...
... Since new material is created at the mid-ocean ridges and Earth is not expanding, somewhere material must be removed from the surface. It turns out that old ocean floor is “subducted” into the mantle at subduction zones. ...
Z SR Midterm Test Review
... Draw and label an example of sea floor spreading in the box below. Be sure to include and label: molten material (magma) convection current motion and direction mid-ocean ridge crust direction direction of rock/crust movement crust, lithosphere, asthenosphere, lower mantle location of ...
... Draw and label an example of sea floor spreading in the box below. Be sure to include and label: molten material (magma) convection current motion and direction mid-ocean ridge crust direction direction of rock/crust movement crust, lithosphere, asthenosphere, lower mantle location of ...
Erosion
... Pacific Plates Pacific plate lies at the bottom of the ocean. Over time, the edges of these plates were forced under the edges of the plates surrounding the ...
... Pacific Plates Pacific plate lies at the bottom of the ocean. Over time, the edges of these plates were forced under the edges of the plates surrounding the ...
Plate Tectonics and Astrobiology
... Life on earth evolved with plate tectonics. Would life elsewhere need it? What does plate tectonics have to do with astrobiology? Plate Tectonics refers to the very slow (few cm per year) movement of ‘plates’ of planetary crust across the surface of the Earth, as well as the effects produced at the ...
... Life on earth evolved with plate tectonics. Would life elsewhere need it? What does plate tectonics have to do with astrobiology? Plate Tectonics refers to the very slow (few cm per year) movement of ‘plates’ of planetary crust across the surface of the Earth, as well as the effects produced at the ...
EARTH`S INTERIOR
... Force of gravity is affected by the _______________ between two masses and the masses of the two objects Gravity Meter (Gravitometer): Measures the gravitational attraction between Earth at a specific location and a mass within the instrument Gravity is Affected by ...
... Force of gravity is affected by the _______________ between two masses and the masses of the two objects Gravity Meter (Gravitometer): Measures the gravitational attraction between Earth at a specific location and a mass within the instrument Gravity is Affected by ...
Plate Tectonic Jeopardy 2011 - cristinscordato
... A force in which the weight of a subducting plate pulls on the rest of the plate. ...
... A force in which the weight of a subducting plate pulls on the rest of the plate. ...
1. Relative dating is using comparison to date rocks or fossils. Law
... 5. The theory of continental drift is Alfred Wegener’s theory that the Earth is made of plates that move, or “drift” over time. The theory suggests the continents were all once together as Pangea. The puzzle-like fit of continents, fossils of plants and animals found at the boundaries of continents ...
... 5. The theory of continental drift is Alfred Wegener’s theory that the Earth is made of plates that move, or “drift” over time. The theory suggests the continents were all once together as Pangea. The puzzle-like fit of continents, fossils of plants and animals found at the boundaries of continents ...
Post-glacial rebound
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Post-glacial rebound (sometimes called continental rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression. Post-glacial rebound and isostatic depression are different parts of a process known as either glacial isostasy, glacial isostatic adjustment, or glacioisostasy. Glacioisostasy is the solid Earth deformation associated with changes in ice mass distribution. The most obvious and direct affects of post-glacial rebound are readily apparent in northern Europe (especially Scotland, Estonia, Latvia, Fennoscandia, and northern Denmark), Siberia, Canada, the Great Lakes of Canada and the United States, the coastal region of the US state of Maine, parts of Patagonia, and Antarctica. However, through processes known as ocean siphoning and continental levering, the effects of post-glacial rebound on sea-level are felt globally far from the locations of current and former ice sheets.